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Stimulating investment in pearl farming in ... - World Fish Center

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Water Temperature and Cyclone Frequency <strong>in</strong> the Pacific: Implications for Pearl Farm<strong>in</strong>g F<strong>in</strong>al, June 2008°C, respectively (Pouvreau and Prasil 2001). The water temperature <strong>in</strong> Mangareva Lagoon,situated even further south and to the east (23° 10’S, 134° 95’W), varies from 21.3 - 28.8 °C(Pouvreau and Prasil 2001). Dur<strong>in</strong>g El Niño years, the water temperature <strong>in</strong> TakapotoLagoon may reach 31.5 °C (Pouvreau et al. 2000b). In November 1985, vertical temperatureprofiles were measured over a 3 day period <strong>in</strong> Rangiroa Lagoon (Rougerie 1985). These<strong>in</strong>dicated that the temperature of the water down to a depth of 30 m was similar to that atthe surface.In other parts of the world, black-lip <strong>pearl</strong> oysters are cultured <strong>in</strong> water with much morevariable temperature regimes. For example, at culture sites at Dongonab Bay, Sudan andKabira Bay, Japan temperatures range from 21 – 34 °C and 17 – 30 °C, respectively (Reed1966; Sugiyama and Tomori 1988).The temperature ranges reported above suggest that black <strong>pearl</strong> farms are either located <strong>in</strong>areas where the water temperature is outside the optimum temperature range or that theoptimum ranges <strong>in</strong> other countries differs markedly from that <strong>in</strong> north-east Australia.2.3.2 Silver Pearl FarmsCSIRO Mar<strong>in</strong>e Research (2003) has compiled coastal ocean temperature statistics for variouslocations off the West Australian coast, <strong>in</strong>clud<strong>in</strong>g two silver-lip <strong>pearl</strong> oyster farms located <strong>in</strong>Roebuck Bay near Broome (18° 2’ S) and Whalebone Island <strong>in</strong> Exmouth Gulf (22° 11’ S),respectively. The mean monthly sea temperature varied from 21.4 °C (July) to 30.9 °C(January) <strong>in</strong> Roebuck Bay and from 19.5 °C (August) to 29.7 °C (February) <strong>in</strong> Exmouth Gulf(Figure 2a). These data are based on measurements taken over different study periods andat different depths (1992 to 1998 near the seabed <strong>in</strong> 12 m of water <strong>in</strong> Roebuck Bay versus1994 to 1998 and 1 m above the seabed <strong>in</strong> about 6 m of water at Whalebone Island) and arenot therefore directly comparable. The water temperature at a silver-lip <strong>pearl</strong> farm <strong>in</strong> KuriBay, Western Australia ranged from 25-32 °C (Pass et al. 1987).The temperature ranges reported above suggest that some Western Australian silver <strong>pearl</strong>farms are located <strong>in</strong> areas where the m<strong>in</strong>imum water temperature is below the lower limit ofthe optimum temperature range and that some are situated <strong>in</strong> areas where the maximumwater temperature is close to the upper limit of the optimum range.2.3.3 Other Locations2.3.3.1 Northern AustraliaCSIRO Mar<strong>in</strong>e Research (2003) has also compiled coastal ocean temperature statistics forthree other locations off the North West Australian coast. The mean sea temperature rangesfor these locations are depicted <strong>in</strong> Figure 2b and are as follows:• Barrow Island (20° 48’ S) - 21.6 °C <strong>in</strong> August to 29.0 °C <strong>in</strong> March, with temperatures at adepth of 15 m similar to those on the surface;• Osprey Bay at N<strong>in</strong>galoo Reef (22° 14’S) - 22.2 °C <strong>in</strong> August to 27.1 °C <strong>in</strong> March at a depthof about 5 m.;• Entrance to Shark Bay (26° 8’S) - 20.9 °C <strong>in</strong> October to 23.8 °C <strong>in</strong> March/April).It should be noted that the temperatures at the entrance to Shark Bay are unlikely to berepresentative of the Bay itself, because of the <strong>in</strong>fluence of strong tidal flows (CSIRO Mar<strong>in</strong>eResearch 2003).The Ecology Lab Pty Ltd – Mar<strong>in</strong>e and Freshwater Studies Page 5

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